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The AAPG/Datapages Combined Publications Database

CSPG Special Publications

Abstract


Canada's Continental Margins and Offshore Petroleum Exploration — Memoir 4, 1975
Pages 205-224
Atlantic Facing Margins

East Greenland Continental Margin

G. L. Johnson, N. J. McMillan, J. Egloff

Abstract

The continental margin of East Greenland consists of a prograded Tertiary sequence overlying Mesozoic and probable Paleozoic strata. On the basis of aeromagnetic data, coast-parallel Mesozoic grabens are believed to be present beneath the continental shelf east of Jameson Land.

In the Late Jurassic, rifting of a pre-existing shallow marine basin commenced. This basin occurs beneath the continental shelves of Norway and Greenland. Fluctuations of sea level, resulting in transgressions and regressions, persisted throughout the Mesozoic. An open seaway between the North Sea and the East Greenland Mesozoic basin apparently existed during Late Permian, Early Jurassic and Cenomanian times. Petroleum prospects appear favorable beneath the Greenland continental shelf.


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